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Tuatara: Volume 15, Issue 3, December 1967

FIG. 3: Development of the Kukri Peneplain Surface (c) on the Post-tectonic Granite, with subsequent deposition of the Beacon Group (horizontal lines) unconformably on the granite. — FIG. 4: The basement geology cf the Dry Valleys today, in a section from east to west. Note the intrusion of dolerite sills (oblique shadings) at three horizons — within the Post-tectonic Grantie, and at the base and middle of the Beacon Group

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FIG. 3: Development of the Kukri Peneplain Surface (c) on the Post-tectonic Granite, with subsequent deposition of the Beacon Group (horizontal lines) unconformably on the granite. FIG. 4: The basement geology cf the Dry Valleys today, in a section from east to west. Note the intrusion of dolerite sills (oblique shadings) at three horizons — within the Post-tectonic Grantie, and at the base and middle of the Beacon Group.

FIG. 3: Development of the Kukri Peneplain Surface (c) on the Post-tectonic Granite, with subsequent deposition of the Beacon Group (horizontal lines) unconformably on the granite.
FIG. 4: The basement geology cf the Dry Valleys today, in a section from east to west. Note the intrusion of dolerite sills (oblique shadings) at three horizons — within the Post-tectonic Grantie, and at the base and middle of the Beacon Group.

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